Earthquakes II: Strain and Faults
Faults
- a large brittle fracture in a rock body
- the point of origin for most earthquakes
Terminology
- movement range along a break in a rock body is fractions of an inch to miles * fractures: fractions of inches to inch movements * faults: feet to mile movements
- contacts between tectonic plates
Normal Fault
- blocks move away from each other
- hanging wall block moves down relative to foot wall
Reverse (or Thrust) Fault
- blocks move towards each other
- hanging wall block moves up relative to foot wall
Strike-Slip Fault
- motion is lateral (like traffic driving)
- fault itself is vertical (no hanging wall or foot wall blocks)
Types of Strike-Slip Faults
- movement relatively to the left
- movement relatively to right
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